What does hydraulic tomography tell us about fractured geological media? A field study and synthetic experiments

Yuanyuan Zha, Tian-Chyi J Yeh, Walter A. Illman, Tatsuya Tanaka, Patrick Bruines, Hironori Onoe, Hiromitsu Saegusa

Research output: Contribution to journalArticle

23 Citations (Scopus)

Abstract

Between 2005 and 2010, Japan Atomic Energy Agency conducted four long-term, independent pumping tests in a fractured granite formation at the Mizunami Underground Research Laboratory (MIU) site in Mizunami city, central Japan. During these tests, drawdowns were monitored at different depths along several deep boreholes. These tests become one of the few, if not the only, hydraulic tomographic survey conducted in the world over thousands of meters in a fractured geologic medium with several fault zones. We analyzed the drawdown-time data set associated with each pumping test independently, and then the data sets from all pumping tests jointly to derive the spatial distributions of hydraulic conductivity (. K) and specific storage (. Ss) of the medium. These estimated distributions revealed some large-scale high K and low K zones. While the low K zones corroborated well with known low permeable layers and fault based on geological investigations, there were no clear geological features that can be related to the large-scale high K zones. In order to understand and substantiate these high and low K zones, we simulated a hydraulic tomographic survey in a synthetic fractured aquifer, which bears similar geologic features (i.e., formations, fractures, and faults) at the MIU site, with exception that the hydraulic properties, fracture and fault distributions were known exactly. Results of the simulation show that not only are the identified high K zones related to fracture networks connected with pumping and observation locations of each pumping test but also their values reflect the degree of connectivity of the network. Afterward, we investigated the extent of the improvement of characterization of the fault and fractures through the use of deploying dense monitoring intervals and late-time flux measurements.

Original languageEnglish (US)
Pages (from-to)17-30
Number of pages14
JournalJournal of Hydrology
Volume531
DOIs
StatePublished - Dec 1 2015

Fingerprint

tomography
pumping
hydraulics
experiment
drawdown
fractured medium
fracture network
geological feature
flux measurement
hydraulic property
field study
test
connectivity
hydraulic conductivity
fault zone
borehole
granite
aquifer
spatial distribution
monitoring

Keywords

  • Fracture and fault hydrogeology
  • Fracture connectivity
  • Hydraulic tomography
  • Inverse modeling

ASJC Scopus subject areas

  • Water Science and Technology

Cite this

What does hydraulic tomography tell us about fractured geological media? A field study and synthetic experiments. / Zha, Yuanyuan; Yeh, Tian-Chyi J; Illman, Walter A.; Tanaka, Tatsuya; Bruines, Patrick; Onoe, Hironori; Saegusa, Hiromitsu.

In: Journal of Hydrology, Vol. 531, 01.12.2015, p. 17-30.

Research output: Contribution to journalArticle

Zha, Yuanyuan ; Yeh, Tian-Chyi J ; Illman, Walter A. ; Tanaka, Tatsuya ; Bruines, Patrick ; Onoe, Hironori ; Saegusa, Hiromitsu. / What does hydraulic tomography tell us about fractured geological media? A field study and synthetic experiments. In: Journal of Hydrology. 2015 ; Vol. 531. pp. 17-30.
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